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Position of the Sun

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31: 2267:. As the graph shows, a sundial can be up to about 16 minutes fast or slow, compared with a clock. Since the Earth rotates at a mean speed of one degree every four minutes, relative to the Sun, this 16-minute displacement corresponds to a shift eastward or westward of about four degrees in the apparent position of the Sun, compared with its mean position. A westward shift causes the sundial to be ahead of the clock. 1375: 2241: 3108: 1804:) is also discouraged for having an error of up to 0.28°. An additional error of up to 0.5° can occur in all equations around the equinoxes if not using a decimal place when selecting N to adjust for the time after UT midnight for the beginning of that day. So the above equation can have up to 2.0° of error, about four times the Sun's angular width, depending on how it is used. 1509:, in early July. This makes processes like the variation of the solar declination happen faster in January than in July. On the graph, this makes the minima more acute than the maxima. Also, since perihelion and aphelion do not happen on the exact dates as the solstices, the maxima and minima are slightly asymmetrical. The rates of change before and after are not quite equal. 1800:−1). The number 10, in (N+10), is the approximate number of days after the December solstice to January 1. This equation overestimates the declination near the September equinox by up to +1.5°. The sine function approximation by itself leads to an error of up to 0.26° and has been discouraged for use in solar energy applications. The 1971 Spencer formula (based on a 3132: 3084: 3120: 3096: 2254:
In addition to the annual north–south oscillation of the Sun's apparent position, corresponding to the variation of its declination described above, there is also a smaller but more complex oscillation in the east–west direction. This is caused by the tilt of the Earth's axis, and also by changes in
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is small, its orbit can be approximated as a circle which causes up to 1° of error. The circle approximation means the EL would be 90° ahead of the solstices in Earth's orbit (at the equinoxes), so that sin(EL) can be written as sin(90+NDS)=cos(NDS) where NDS is the number of days after the December
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of light in the atmosphere, which causes the apparent angle of elevation of the Sun as seen by an observer to be higher than the actual angle of elevation, especially at low Sun elevations. For example, when the Sun is at an elevation of 10°, it appears to be at 10.1°. The Sun's declination can be
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More complicated algorithms correct for changes to the ecliptic longitude by using terms in addition to the 1st-order eccentricity correction above. They also correct the 23.44° obliquity which changes very slightly with time. Corrections may also include the effects of the moon in offsetting the
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by astronomers) is the angle between the Earth's axis and a line perpendicular to the Earth's orbit. The Earth's axial tilt changes slowly over thousands of years but its current value of about ε = 23°44' is nearly constant, so the change in solar declination during one year is nearly the same as
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If the 90° axial tilt is decreased, then the absolute maximum and minimum values of the declination would decrease, to equal the axial tilt. Also, the shapes of the maxima and minima on the graph would become less acute, being curved to resemble the maxima and minima of a sine wave. However, even
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Zhang, T., Stackhouse, P.W., Macpherson, B., and Mikovitz, J.C., 2021. A solar azimuth formula that renders circumstantial treatment unnecessary without compromising mathematical rigor: Mathematical setup, application and extension of a formula based on the subsolar point and atan2 function.
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of the Earth's orbit. The eccentricity varies very slowly over time, but for dates fairly close to the present, it can be considered to be constant. The largest errors in this equation are less than ± 0.2°, but are less than ± 0.03° for a given year if the number 10 is adjusted up or down in
2339:, plotted horizontally. Usually, the scales are chosen so that equal distances on the diagram represent equal angles in both directions on the celestial sphere. Thus 4 minutes (more precisely 3 minutes, 56 seconds), in the equation of time, are represented by the same distance as 1° in the 2195:
fractional days as determined by how far the previous year's December solstice occurred before or after noon on December 22. These accuracies are compared to NOAA's advanced calculations which are based on the 1999 Jean Meeus algorithm that is accurate to within 0.01°.
2274:, using the word "equation" in a somewhat archaic sense meaning "correction". The oscillation is measured in units of time, minutes and seconds, corresponding to the amount that a sundial would be ahead of a clock. The equation of time can be positive or negative. 2214:
is applied, which depends on the observer's distance away from the center of the Earth. This correction is less than 0.0025°. The error in calculating the position of the center of the Sun can be less than 0.00015°. For comparison, the Sun's width is about 0.5°.
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with time. Eventually, the Sun would be directly above the South Pole, with a declination of −90°; then it would start to move northward at a constant speed. Thus, the graph of solar declination, as seen from this highly tilted Earth, would resemble a
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the speed of its orbital motion around the Sun produced by the elliptical shape of the orbit. The principal effects of this east–west oscillation are variations in the timing of events such as sunrise and sunset, and in the reading of a
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Some analemmas are marked to show the position of the Sun on the graph on various dates, a few days apart, throughout the year. This enables the analemma to be used to make simple analog computations of quantities such as the times and
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The path of the Sun over the celestial sphere through the course of the day for an observer at 56°N latitude. The Sun's path changes with its declination during the year. The intersections of the curves with the horizontal axis show
1071: 612: 1787: 787: 1134: 952: 722: 434: 375: 2177: 2016: 1671: 1278: 1233: 312: 1188: 2186:−1) and can include decimals to adjust for local times later or earlier in the day. The number 2, in (N-2), is the approximate number of days after January 1 to the Earth's 890: 996: 814: 648: 972: 1512:
The graph of apparent solar declination is therefore different in several ways from a sine wave. Calculating it accurately involves some complexity, as shown below.
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Earth's position from the center of the pair's orbit around the Sun. After obtaining the declination relative to the center of the Earth, a further correction for
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The declination can be more accurately calculated by not making the two approximations, using the parameters of the Earth's orbit to more accurately estimate EL:
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The equation of time — above the axis a sundial will appear fast relative to a clock showing local mean time, and below the axis a sundial will appear slow.
1008: 2803: 2904: 3157: 2629: 2324:, which resembles a figure-8. An analemma can be pictured by superimposing photographs taken at the same time of day, a few days apart for a 544: 176:, for the observer's local time and location. This is the coordinate system normally used to calculate the position of the Sun in terms of 2861: 2833: 1691: 2693: 2517: 743: 2320:
is also occasionally, but rarely, used in other contexts.) It can be considered as an image of the Sun's apparent motion during a
2232:, to calculate its azimuth and also its true elevation, which can then be corrected for refraction to give its apparent position. 1086: 904: 266:, the number of days (positive or negative, including fractional days) since Greenwich noon, Terrestrial Time, on 1 January 2000 ( 30: 3008: 1685:
solstice. By also using the approximation that arcsin is close to d·cos(NDS), the following frequently used formula is obtained:
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of the Sun (actually, of the Earth in its orbit around the Sun, but it is convenient to pretend the Sun orbits the Earth), is:
1544:, the angle between the rays of the Sun and the plane of the Earth's equator reaches its maximum value of 23°44'. Therefore, δ 2418: 2423: 668: 390: 331: 1490:
when the axial tilt equals that of the actual Earth, the maxima and minima remain more acute than those of a sine wave.
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To find the Sun's position for a given location at a given time, one may therefore proceed in three steps as follows:
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To get RA at the right quadrant on computer programs use double argument Arctan function such as ATAN2(y,x)
2652: 247:, to a precision of about 0°.01 (36″), for dates between 1950 and 2050. Similar equations are coded into a 2224: 480: 2749: 2433: 2903:
Blanco-Muriel, Manuel; Alarcón-Padilla, Diego C; López-Moratalla, Teodoro; Lara-Coira, Martín (2001).
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Sproul, Alistair B. (2007). "Derivation of the solar geometric relationships using vector analysis".
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of the Sun never exceeds 0.00033° (a little over 1″), and the distance of the Sun from the Earth, in
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of 23.44°, but one lobe of the wave is several days longer than the other, among other differences.
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We see light from the Sun about 20 angle seconds from where the Sun is when the light is seen. See
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N is the number of days since midnight UT as January 1 begins (i.e. the days part of the
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U.S. Naval Observatory; U.K. Hydrographic Office, H.M. Nautical Almanac Office (2008).
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An analemma is drawn as it would be seen in the sky by an observer looking upward. If
17: 3146: 3067: 2584: 2576: 2321: 2198:(The above formula is related to a reasonably simple and accurate calculation of the 1479: 1446: 1408: 1396: 1327: 35: 2682:
U.S. Naval Observatory Nautical Almanac Office (1992). P. Kenneth Seidelmann (ed.).
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around the Sun, and if its axis were tilted 90°, so that the axis itself is on the
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website. Positions of Solar System objects based on the INPOP series ephemerides.
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Much the same set of equations, covering the years 1800 to 2200, can be found at
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between plus and minus 90°, with linear segments between the maxima and minima.
1415:, when its value is the negative of the axial tilt. This variation produces the 1400: 1374: 1077: 271: 209: 205: 140: 110: 2606: 2240: 2223:
The declination calculations described above do not include the effects of the
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is a diagram that shows the annual variation of the Sun's position on the
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Since the main effect of this oscillation concerns time, it is called the
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website. Very accurate positions of Solar System objects based on the
2379: 1483: 1454: 1450: 1416: 607:{\displaystyle \lambda =L+1.915^{\circ }\sin g+0.020^{\circ }\sin 2g} 3047: 3043: 2282: 1680:(essentially, the Earth's position in its orbit). Since the Earth's 3095: 27:
Calculating the Sun's location in the sky at a given time and place
2659:. Graphs of the error of these equations, compared to an accurate 2559: 2366:, on which the continents, etc., are shown with west to the left. 2363: 2351: 2281: 2260: 2239: 1373: 94: 29: 1473:
at a constant rate, so that the solar declination would decrease
1461:, so its declination would be +90°. For the next few months, the 3032: 2649: 2355: 2325: 1782:{\displaystyle \delta _{\odot }=-23.44^{\circ }\cdot \cos \left} 106: 86: 3025:. An interactive calculator showing the Sun's path in the sky. 2332: 1792:
where N is the day of the year beginning with N=0 at midnight
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at a mean speed of 1° every 4 minutes, relative to the Sun.
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The Sun's declination at any given moment is calculated by:
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The following phenomena would occur if Earth were a perfect
1129:{\displaystyle \delta =\arcsin(\sin \epsilon \sin \lambda )} 947:{\displaystyle \alpha =\arctan(\cos \epsilon \tan \lambda )} 2947:"Solar Position Algorithm for Solar Radiation Applications" 239:, can be used to calculate the apparent coordinates of the 2742:"Fourier series representation of the position of the sun" 2688:. University Science Books, Mill Valley, CA. p. 12. 1387:
The Sun appears to move northward during the northern
717:{\displaystyle R=1.00014-0.01671\cos g-0.00014\cos 2g} 429:{\displaystyle g=357.528^{\circ }+0.9856003^{\circ }n} 370:{\displaystyle L=280.460^{\circ }+0.9856474^{\circ }n} 131:, so that the Sun appears to move across the sky in a 3072: 2508:(1991). "Chapter 12: Transformation of Coordinates". 2331:
An analemma can also be considered as a graph of the
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which can be simplified by evaluating constants to:
1796:(UT) as January 1 begins (i.e. the days part of the 1559:, the center of the Sun appears to pass through the 3031:, at the NOAA Earth System Research Laboratories's 1426:of the Sun's declination during a year resembles a 1383:
in degrees from North where the Sun rises and sets.
737:is not obtained elsewhere, it can be approximated: 184:, and the two parameters can be used to depict the 2685:Explanatory Supplement to the Astronomical Almanac 2171: 2010: 1781: 1665: 1342: 1318: 1294: 1272: 1227: 1182: 1128: 1065: 990: 966: 946: 884: 848: 828: 808: 781: 716: 642: 606: 519: 499: 471: 451: 428: 369: 306: 1403:reaches a maximum equal to the angle of Earth's 479:in the range 0° to 360° by adding or subtracting 251:90 routine in Ref. and are used to calculate the 2190:. The number 0.0167 is the current value of the 2975:National Oceanic and Atmospheric Administration 2477:, the Earth's orbit would be stated as being a 2172:{\displaystyle \delta _{\odot }=-\arcsin \left} 1548:= +23°44' at the northern summer solstice and δ 1501:. Earth moves more rapidly around the Sun near 3058:General ephemerides of the solar system bodies 3039:NOAA's declination and sun position calculator 2011:{\displaystyle \delta _{\odot }=\arcsin \left} 1666:{\displaystyle \delta _{\odot }=\arcsin \left} 1273:{\displaystyle Z=R\sin \epsilon \sin \lambda } 1228:{\displaystyle Y=R\cos \epsilon \sin \lambda } 109:, the Sun appears to move with respect to the 2727:"Selected Astronomical Constants, 2015 (TXT)" 2710:"Selected Astronomical Constants, 2015 (PDF)" 1453:). At one date in the year, the Sun would be 8: 3011:, at National Renewable Energy Laboratory's 2729:. US Naval Observatory. 2014. p. K6–K7. 2715:. US Naval Observatory. 2014. p. K6–K7. 2607:https://doi.org/10.1016/j.renene.2021.03.047 2852: 2850: 2596: 2594: 1552:= −23°44' at the southern summer solstice. 259:as observed from the surface of the Earth. 2624:. U.S. Govt. Printing Office. p. C5. 2621:The Astronomical Almanac for the Year 2010 2335:, usually plotted vertically, against the 1370:Declination of the Sun as seen from Earth 135:that depends on the observer's geographic 2558: 2545:(2013). "The Sun's position in the sky". 2537: 2535: 2533: 2531: 2529: 2129: 2108: 2076: 2035: 2029: 1963: 1957: 1929: 1923: 1890: 1884: 1859: 1821: 1815: 1741: 1735: 1715: 1699: 1693: 1622: 1584: 1578: 1335: 1311: 1287: 1241: 1196: 1160: 1088: 1010: 983: 959: 906: 877: 841: 821: 801: 770: 757: 745: 670: 629: 586: 564: 546: 512: 492: 464: 444: 417: 404: 392: 358: 345: 333: 307:{\displaystyle n=\mathrm {JD} -2451545.0} 290: 282: 3079: 2497: 2466: 2971:"Atmospheric Refraction Approximation" 2758: 2747: 1148:rectangular equatorial coordinates in 7: 2512:. Richmond, VA: Willmann Bell, Inc. 274:for the desired time is known, then 158:calculate the Sun's position in the 3068:Solar position in R. Insol package. 2945:Ibrahim Reda & Afshin Andreas. 117:, along a circular path called the 2862:Earth System Research Laboratories 2834:Earth System Research Laboratories 1141:Rectangular equatorial coordinates 294: 291: 73:a.m. local time on a March morning 25: 245:mean equinox and ecliptic of date 3130: 3118: 3106: 3094: 3082: 1469:at constant speed, crossing the 1302:axis is in the direction of the 1183:{\displaystyle X=R\cos \lambda } 856:form a complete position of the 864:. This can be converted to the 3013:Renewable Resource Data Center 2650:U.S. Naval Observatory website 2419:Effect of Sun angle on climate 1505:, in early January, than near 1123: 1102: 1060: 1027: 941: 920: 321:of the Sun, corrected for the 192:This calculation is useful in 1: 2932:10.1016/s0038-092x(00)00156-0 2646:Approximate Solar Coordinates 3158:Dynamics of the Solar System 2905:"Computing the Solar Vector" 2790:10.1016/j.renene.2006.05.001 1365:Horizontal coordinate system 866:equatorial coordinate system 527:are really to be evaluated ( 174:horizontal coordinate system 167:equatorial coordinate system 2858:"Solar Calculation Details" 2547:European Journal of Physics 2424:Newcomb's Tables of the Sun 3174: 3033:Global Monitoring Division 2577:10.1088/0143-0807/34/3/633 2354:is shown at the top, then 2301: 2247: 1407:(23.44° or 23°26') on the 1362: 862:ecliptic coordinate system 233:These equations, from the 160:ecliptic coordinate system 147:depends on the geographic 85:is a function of both the 2883:"Astronomical Algorithms" 1534:obliquity of the ecliptic 1482:rather than a sine wave, 885:{\displaystyle \epsilon } 870:obliquity of the ecliptic 735:obliquity of the ecliptic 729:Obliquity of the ecliptic 487:— which is to say, 3009:Solar Position Algorithm 991:{\displaystyle \lambda } 809:{\displaystyle \lambda } 643:{\displaystyle \beta =0} 139:. The time when the Sun 3019:Sun Position Calculator 2830:"NOAA Solar Calculator" 2605:, 172, 1333-1340. DOI: 2510:Astronomical Algorithms 2409:Solar annual aberration 2396:Solar annual aberration 1520:The declination of the 967:{\displaystyle \alpha } 2757:Cite journal requires 2740:J. W. Spencer (1971). 2299: 2245: 2219:Atmospheric refraction 2173: 2012: 1783: 1667: 1555:At the moment of each 1537:during the next year. 1465:would move toward the 1384: 1359:Horizontal coordinates 1344: 1320: 1296: 1274: 1229: 1184: 1130: 1067: 992: 968: 948: 886: 850: 830: 829:{\displaystyle \beta } 810: 793:Equatorial coordinates 783: 718: 644: 621:of the Sun is nearly: 608: 521: 501: 473: 453: 430: 371: 308: 127:about its axis causes 74: 18:Declination of the Sun 3029:NOAA Solar Calculator 2663:, can also be viewed. 2434:Solar elevation angle 2285: 2243: 2228:used, along with its 2202:, which is described 2174: 2013: 1784: 1668: 1377: 1363:Further information: 1345: 1321: 1297: 1275: 1230: 1185: 1131: 1068: 993: 969: 949: 887: 851: 831: 811: 784: 719: 645: 609: 522: 502: 474: 454: 431: 372: 309: 262:Start by calculating 105:over the course of a 33: 2672:Meeus (1991), p. 152 2483:orbital eccentricity 2028: 1814: 1692: 1682:orbital eccentricity 1577: 1352:North celestial pole 1334: 1310: 1286: 1240: 1195: 1159: 1087: 1009: 982: 958: 905: 876: 840: 820: 800: 744: 669: 628: 545: 511: 491: 463: 443: 391: 332: 281: 236:Astronomical Almanac 229:Ecliptic coordinates 224:Approximate position 2924:2001SoEn...70..431B 2569:2013EJPh...34..633J 2475:celestial mechanics 2429:Solar azimuth angle 1471:circles of latitude 892:, and continuing: 868:by calculating the 323:aberration of light 257:solar azimuth angle 182:solar azimuth angle 91:geographic location 79:position of the Sun 53: /  2995:Sundial#Noon marks 2655:2016-01-31 at the 2543:Jenkins, Alejandro 2390:Light-time effects 2300: 2298:to the same scale 2246: 2169: 2008: 1779: 1678:ecliptic longitude 1663: 1385: 1340: 1316: 1292: 1270: 1225: 1180: 1150:astronomical units 1126: 1063: 988: 964: 944: 882: 846: 826: 806: 779: 714: 660:astronomical units 640: 604: 536:ecliptic longitude 517: 497: 469: 449: 426: 367: 304: 253:solar zenith angle 178:solar zenith angle 93:of observation on 75: 2631:978-0-7077-4082-9 2333:Sun's declination 1972: 1938: 1899: 1750: 1561:celestial equator 1455:directly overhead 1413:December solstice 1393:celestial equator 1350:axis towards the 1343:{\displaystyle Z} 1319:{\displaystyle Y} 1295:{\displaystyle X} 849:{\displaystyle R} 656:ecliptic latitude 619:ecliptic latitude 520:{\displaystyle g} 500:{\displaystyle L} 483:of 360° as needed 472:{\displaystyle g} 452:{\displaystyle L} 16:(Redirected from 3165: 3135: 3134: 3133: 3123: 3122: 3121: 3111: 3110: 3109: 3099: 3098: 3087: 3086: 3085: 3078: 2997: 2992: 2986: 2985: 2983: 2981: 2967: 2961: 2960: 2958: 2956: 2951: 2942: 2936: 2935: 2909: 2900: 2894: 2893: 2891: 2889: 2879: 2873: 2872: 2870: 2868: 2854: 2845: 2844: 2842: 2840: 2826: 2820: 2819: 2817: 2815: 2806:. Archived from 2800: 2794: 2793: 2784:(7): 1187–1205. 2778:Renewable Energy 2773: 2767: 2766: 2760: 2755: 2753: 2745: 2737: 2731: 2730: 2723: 2717: 2716: 2714: 2706: 2700: 2699: 2679: 2673: 2670: 2664: 2642: 2636: 2635: 2615: 2609: 2603:Renewable Energy 2598: 2589: 2588: 2562: 2539: 2524: 2523: 2502: 2486: 2471: 2454:Sunrise equation 2439:Solar irradiance 2337:equation of time 2314:celestial sphere 2296:equation of time 2272:equation of time 2259:compared with a 2250:Equation of time 2236:Equation of time 2200:Equation of Time 2178: 2176: 2175: 2170: 2168: 2164: 2163: 2159: 2158: 2154: 2153: 2149: 2134: 2133: 2113: 2112: 2100: 2096: 2081: 2080: 2040: 2039: 2017: 2015: 2014: 2009: 2007: 2003: 2002: 1998: 1997: 1993: 1992: 1988: 1973: 1968: 1967: 1958: 1939: 1934: 1933: 1924: 1919: 1915: 1900: 1895: 1894: 1885: 1869: 1865: 1864: 1863: 1826: 1825: 1788: 1786: 1785: 1780: 1778: 1774: 1773: 1769: 1751: 1746: 1745: 1736: 1720: 1719: 1704: 1703: 1676:where EL is the 1672: 1670: 1669: 1664: 1662: 1658: 1657: 1653: 1632: 1628: 1627: 1626: 1589: 1588: 1349: 1347: 1346: 1341: 1325: 1323: 1322: 1317: 1301: 1299: 1298: 1293: 1279: 1277: 1276: 1271: 1234: 1232: 1231: 1226: 1189: 1187: 1186: 1181: 1135: 1133: 1132: 1127: 1072: 1070: 1069: 1064: 997: 995: 994: 989: 973: 971: 970: 965: 953: 951: 950: 945: 891: 889: 888: 883: 855: 853: 852: 847: 835: 833: 832: 827: 815: 813: 812: 807: 788: 786: 785: 780: 775: 774: 762: 761: 723: 721: 720: 715: 649: 647: 646: 641: 613: 611: 610: 605: 591: 590: 569: 568: 526: 524: 523: 518: 506: 504: 503: 498: 486: 478: 476: 475: 470: 458: 456: 455: 450: 435: 433: 432: 427: 422: 421: 409: 408: 376: 374: 373: 368: 363: 362: 350: 349: 313: 311: 310: 305: 297: 125:Earth's rotation 115:celestial sphere 72: 68: 67: 65: 64: 63: 58: 57:8.283°N 98.600°E 54: 51: 50: 49: 46: 21: 3173: 3172: 3168: 3167: 3166: 3164: 3163: 3162: 3143: 3142: 3141: 3131: 3129: 3119: 3117: 3107: 3105: 3093: 3083: 3081: 3073: 3044:HORIZONS System 3023:pveducation.org 3005: 3000: 2993: 2989: 2979: 2977: 2969: 2968: 2964: 2954: 2952: 2949: 2944: 2943: 2939: 2907: 2902: 2901: 2897: 2887: 2885: 2881: 2880: 2876: 2866: 2864: 2856: 2855: 2848: 2838: 2836: 2828: 2827: 2823: 2813: 2811: 2810:on 9 March 2012 2802: 2801: 2797: 2775: 2774: 2770: 2756: 2746: 2739: 2738: 2734: 2725: 2724: 2720: 2712: 2708: 2707: 2703: 2696: 2681: 2680: 2676: 2671: 2667: 2657:Wayback Machine 2643: 2639: 2632: 2617: 2616: 2612: 2599: 2592: 2541: 2540: 2527: 2520: 2504: 2503: 2499: 2495: 2490: 2489: 2485:of less than 1. 2472: 2468: 2463: 2458: 2404: 2392: 2306: 2280: 2265:local mean time 2252: 2238: 2230:right ascension 2221: 2139: 2135: 2125: 2124: 2120: 2104: 2086: 2082: 2072: 2071: 2067: 2057: 2053: 2031: 2026: 2025: 1978: 1974: 1959: 1956: 1952: 1925: 1905: 1901: 1886: 1883: 1879: 1855: 1851: 1847: 1840: 1836: 1817: 1812: 1811: 1759: 1755: 1737: 1734: 1730: 1711: 1695: 1690: 1689: 1646: 1642: 1618: 1614: 1610: 1603: 1599: 1580: 1575: 1574: 1566: 1551: 1547: 1527: 1518: 1391:, crossing the 1372: 1367: 1361: 1332: 1331: 1308: 1307: 1284: 1283: 1238: 1237: 1193: 1192: 1157: 1156: 1143: 1085: 1084: 1007: 1006: 980: 979: 974:is in the same 956: 955: 903: 902: 896:Right ascension 874: 873: 838: 837: 818: 817: 798: 797: 795: 766: 753: 742: 741: 731: 667: 666: 626: 625: 582: 560: 543: 542: 538:of the Sun is: 509: 508: 489: 488: 484: 461: 460: 441: 440: 413: 400: 389: 388: 354: 341: 330: 329: 279: 278: 231: 226: 172:convert to the 165:convert to the 143:the observer's 97:'s surface. As 70: 61: 59: 55: 52: 47: 44: 42: 40: 39: 28: 23: 22: 15: 12: 11: 5: 3171: 3169: 3161: 3160: 3155: 3145: 3144: 3140: 3139: 3127: 3115: 3103: 3091: 3071: 3070: 3065: 3055: 3041: 3036: 3026: 3016: 3004: 3003:External links 3001: 2999: 2998: 2987: 2962: 2937: 2918:(5): 431–441. 2895: 2874: 2846: 2821: 2795: 2768: 2759:|journal= 2732: 2718: 2701: 2694: 2674: 2665: 2637: 2630: 2610: 2590: 2553:(3): 633–652. 2525: 2518: 2496: 2494: 2491: 2488: 2487: 2465: 2464: 2462: 2459: 2457: 2456: 2451: 2446: 2441: 2436: 2431: 2426: 2421: 2416: 2411: 2405: 2403: 2400: 2391: 2388: 2302:Main article: 2279: 2276: 2248:Main article: 2237: 2234: 2220: 2217: 2180: 2179: 2167: 2162: 2157: 2152: 2148: 2145: 2142: 2138: 2132: 2128: 2123: 2119: 2116: 2111: 2107: 2103: 2099: 2095: 2092: 2089: 2085: 2079: 2075: 2070: 2066: 2063: 2060: 2056: 2052: 2049: 2046: 2043: 2038: 2034: 2019: 2018: 2006: 2001: 1996: 1991: 1987: 1984: 1981: 1977: 1971: 1966: 1962: 1955: 1951: 1948: 1945: 1942: 1937: 1932: 1928: 1922: 1918: 1914: 1911: 1908: 1904: 1898: 1893: 1889: 1882: 1878: 1875: 1872: 1868: 1862: 1858: 1854: 1850: 1846: 1843: 1839: 1835: 1832: 1829: 1824: 1820: 1802:Fourier series 1794:Universal Time 1790: 1789: 1777: 1772: 1768: 1765: 1762: 1758: 1754: 1749: 1744: 1740: 1733: 1729: 1726: 1723: 1718: 1714: 1710: 1707: 1702: 1698: 1674: 1673: 1661: 1656: 1652: 1649: 1645: 1641: 1638: 1635: 1631: 1625: 1621: 1617: 1613: 1609: 1606: 1602: 1598: 1595: 1592: 1587: 1583: 1564: 1549: 1545: 1525: 1517: 1514: 1463:subsolar point 1443:circular orbit 1371: 1368: 1360: 1357: 1356: 1355: 1339: 1315: 1291: 1280: 1269: 1266: 1263: 1260: 1257: 1254: 1251: 1248: 1245: 1235: 1224: 1221: 1218: 1215: 1212: 1209: 1206: 1203: 1200: 1190: 1179: 1176: 1173: 1170: 1167: 1164: 1142: 1139: 1138: 1137: 1125: 1122: 1119: 1116: 1113: 1110: 1107: 1104: 1101: 1098: 1095: 1092: 1074: 1073: 1062: 1059: 1056: 1053: 1050: 1047: 1044: 1041: 1038: 1035: 1032: 1029: 1026: 1023: 1020: 1017: 1014: 1000: 999: 987: 963: 943: 940: 937: 934: 931: 928: 925: 922: 919: 916: 913: 910: 881: 845: 825: 805: 794: 791: 790: 789: 778: 773: 769: 765: 760: 756: 752: 749: 730: 727: 726: 725: 713: 710: 707: 704: 701: 698: 695: 692: 689: 686: 683: 680: 677: 674: 652: 651: 639: 636: 633: 615: 614: 603: 600: 597: 594: 589: 585: 581: 578: 575: 572: 567: 563: 559: 556: 553: 550: 516: 496: 468: 448: 437: 436: 425: 420: 416: 412: 407: 403: 399: 396: 378: 377: 366: 361: 357: 353: 348: 344: 340: 337: 319:mean longitude 315: 314: 303: 300: 296: 293: 289: 286: 230: 227: 225: 222: 190: 189: 170: 163: 129:diurnal motion 26: 24: 14: 13: 10: 9: 6: 4: 3: 2: 3170: 3159: 3156: 3154: 3151: 3150: 3148: 3138: 3128: 3126: 3116: 3114: 3104: 3102: 3097: 3092: 3090: 3080: 3076: 3069: 3066: 3063: 3059: 3056: 3053: 3052:JPL DE series 3049: 3045: 3042: 3040: 3037: 3034: 3030: 3027: 3024: 3020: 3017: 3014: 3010: 3007: 3006: 3002: 2996: 2991: 2988: 2976: 2972: 2966: 2963: 2948: 2941: 2938: 2933: 2929: 2925: 2921: 2917: 2913: 2906: 2899: 2896: 2884: 2878: 2875: 2863: 2859: 2853: 2851: 2847: 2835: 2831: 2825: 2822: 2809: 2805: 2799: 2796: 2791: 2787: 2783: 2779: 2772: 2769: 2764: 2751: 2743: 2736: 2733: 2728: 2722: 2719: 2711: 2705: 2702: 2697: 2695:0-935702-68-7 2691: 2687: 2686: 2678: 2675: 2669: 2666: 2662: 2658: 2654: 2651: 2647: 2641: 2638: 2633: 2627: 2623: 2622: 2614: 2611: 2608: 2604: 2597: 2595: 2591: 2586: 2582: 2578: 2574: 2570: 2566: 2561: 2556: 2552: 2548: 2544: 2538: 2536: 2534: 2532: 2530: 2526: 2521: 2519:0-943396-35-2 2515: 2511: 2507: 2501: 2498: 2492: 2484: 2480: 2476: 2470: 2467: 2460: 2455: 2452: 2450: 2447: 2445: 2442: 2440: 2437: 2435: 2432: 2430: 2427: 2425: 2422: 2420: 2417: 2415: 2412: 2410: 2407: 2406: 2401: 2399: 2397: 2389: 2387: 2385: 2381: 2377: 2373: 2367: 2365: 2361: 2357: 2353: 2348: 2346: 2345:Earth rotates 2342: 2338: 2334: 2329: 2327: 2323: 2319: 2315: 2311: 2305: 2297: 2293: 2289: 2284: 2277: 2275: 2273: 2268: 2266: 2262: 2258: 2251: 2242: 2235: 2233: 2231: 2226: 2218: 2216: 2213: 2207: 2205: 2201: 2196: 2193: 2189: 2185: 2165: 2160: 2155: 2150: 2146: 2143: 2140: 2136: 2130: 2126: 2121: 2117: 2114: 2109: 2105: 2101: 2097: 2093: 2090: 2087: 2083: 2077: 2073: 2068: 2064: 2061: 2058: 2054: 2050: 2047: 2044: 2041: 2036: 2032: 2024: 2023: 2022: 2004: 1999: 1994: 1989: 1985: 1982: 1979: 1975: 1969: 1964: 1960: 1953: 1949: 1946: 1943: 1940: 1935: 1930: 1926: 1920: 1916: 1912: 1909: 1906: 1902: 1896: 1891: 1887: 1880: 1876: 1873: 1870: 1866: 1860: 1856: 1852: 1848: 1844: 1841: 1837: 1833: 1830: 1827: 1822: 1818: 1810: 1809: 1808: 1805: 1803: 1799: 1795: 1775: 1770: 1766: 1763: 1760: 1756: 1752: 1747: 1742: 1738: 1731: 1727: 1724: 1721: 1716: 1712: 1708: 1705: 1700: 1696: 1688: 1687: 1686: 1683: 1679: 1659: 1654: 1650: 1647: 1643: 1639: 1636: 1633: 1629: 1623: 1619: 1615: 1611: 1607: 1604: 1600: 1596: 1593: 1590: 1585: 1581: 1573: 1572: 1571: 1568: 1562: 1558: 1553: 1543: 1538: 1535: 1531: 1523: 1515: 1513: 1510: 1508: 1504: 1500: 1496: 1495:Earth's orbit 1491: 1487: 1485: 1481: 1480:triangle wave 1476: 1472: 1468: 1464: 1460: 1456: 1452: 1448: 1447:orbital plane 1444: 1440: 1435: 1433: 1429: 1425: 1420: 1418: 1414: 1410: 1409:June solstice 1406: 1402: 1398: 1397:March equinox 1394: 1390: 1382: 1376: 1369: 1366: 1358: 1353: 1337: 1329: 1328:June Solstice 1326:axis towards 1313: 1305: 1304:March equinox 1289: 1281: 1267: 1264: 1261: 1258: 1255: 1252: 1249: 1246: 1243: 1236: 1222: 1219: 1216: 1213: 1210: 1207: 1204: 1201: 1198: 1191: 1177: 1174: 1171: 1168: 1165: 1162: 1155: 1154: 1153: 1151: 1147: 1140: 1120: 1117: 1114: 1111: 1108: 1105: 1099: 1096: 1093: 1090: 1083: 1082: 1081: 1079: 1057: 1054: 1051: 1048: 1045: 1042: 1039: 1036: 1033: 1030: 1024: 1021: 1018: 1015: 1012: 1005: 1004: 1003: 985: 977: 961: 938: 935: 932: 929: 926: 923: 917: 914: 911: 908: 901: 900: 899: 897: 893: 879: 871: 867: 863: 859: 843: 823: 803: 792: 776: 771: 767: 763: 758: 754: 750: 747: 740: 739: 738: 736: 728: 711: 708: 705: 702: 699: 696: 693: 690: 687: 684: 681: 678: 675: 672: 665: 664: 663: 661: 657: 637: 634: 631: 624: 623: 622: 620: 601: 598: 595: 592: 587: 583: 579: 576: 573: 570: 565: 561: 557: 554: 551: 548: 541: 540: 539: 537: 534:Finally, the 532: 530: 514: 494: 482: 466: 446: 423: 418: 414: 410: 405: 401: 397: 394: 387: 386: 385: 383: 364: 359: 355: 351: 346: 342: 338: 335: 328: 327: 326: 324: 320: 301: 298: 287: 284: 277: 276: 275: 273: 269: 265: 260: 258: 254: 250: 246: 242: 238: 237: 228: 223: 221: 219: 215: 211: 207: 203: 199: 195: 187: 183: 179: 175: 171: 168: 164: 161: 157: 156: 155: 152: 150: 146: 142: 138: 134: 130: 126: 122: 120: 116: 112: 108: 104: 100: 96: 92: 88: 84: 80: 66: 62:8.283; 98.600 38:in Thailand ( 37: 36:Phang Nga Bay 34:The Sun over 32: 19: 3137:Solar System 3054:ephemerides. 2990: 2978:. Retrieved 2965: 2953:. Retrieved 2940: 2915: 2912:Solar Energy 2911: 2898: 2886:. Retrieved 2877: 2865:. Retrieved 2837:. Retrieved 2824: 2812:. Retrieved 2808:the original 2798: 2781: 2777: 2771: 2750:cite journal 2735: 2721: 2704: 2684: 2677: 2668: 2640: 2620: 2613: 2602: 2550: 2546: 2509: 2500: 2479:Kepler orbit 2469: 2393: 2368: 2359: 2349: 2330: 2317: 2307: 2271: 2269: 2253: 2222: 2208: 2197: 2192:eccentricity 2184:ordinal date 2181: 2020: 1806: 1798:ordinal date 1791: 1675: 1569: 1554: 1539: 1533: 1532:(called the 1519: 1516:Calculations 1511: 1493:In reality, 1492: 1488: 1474: 1449:(similar to 1436: 1421: 1386: 1146:Right-handed 1144: 1075: 1001: 894: 796: 732: 653: 616: 533: 438: 382:mean anomaly 379: 316: 263: 261: 234: 232: 214:solar energy 191: 153: 123: 99:Earth orbits 78: 76: 3125:Outer space 3113:Spaceflight 2980:28 February 2955:28 February 2888:28 February 2867:28 February 2839:28 February 2814:28 February 2506:Meeus, Jean 2341:declination 2292:declination 2290:with solar 1401:declination 1078:declination 272:Julian date 210:climatology 206:meteorology 111:fixed stars 60: / 3147:Categories 2804:"SunAlign" 2493:References 2444:Solar time 2358:is to the 2225:refraction 2188:perihelion 1530:axial tilt 1503:perihelion 1499:elliptical 1484:zigzagging 1467:South Pole 1459:North Pole 1424:line graph 1405:axial tilt 1330:, and the 733:Where the 270:). If the 198:navigation 69:), at 7:00 3089:Astronomy 3060:, at the 3046:, at the 2661:ephemeris 2648:, at the 2585:119282288 2560:1208.1043 2144:− 2131:∘ 2118:⁡ 2110:∘ 2078:∘ 2065:⁡ 2051:⁡ 2045:− 2037:⊙ 2033:δ 1983:− 1965:∘ 1950:⁡ 1941:⋅ 1936:π 1931:∘ 1892:∘ 1877:⁡ 1871:⋅ 1861:∘ 1853:− 1845:⁡ 1834:⁡ 1823:⊙ 1819:δ 1753:⋅ 1743:∘ 1728:⁡ 1722:⋅ 1717:∘ 1709:− 1701:⊙ 1697:δ 1640:⁡ 1634:⋅ 1624:∘ 1616:− 1608:⁡ 1597:⁡ 1586:⊙ 1582:δ 1542:solstices 1432:amplitude 1428:sine wave 1268:λ 1265:⁡ 1259:ϵ 1256:⁡ 1223:λ 1220:⁡ 1214:ϵ 1211:⁡ 1178:λ 1175:⁡ 1121:λ 1118:⁡ 1112:ϵ 1109:⁡ 1100:⁡ 1091:δ 1058:λ 1055:⁡ 1046:λ 1043:⁡ 1037:ϵ 1034:⁡ 1022:⁡ 1013:α 986:λ 962:α 939:λ 936:⁡ 930:ϵ 927:⁡ 918:⁡ 909:α 880:ϵ 824:β 804:λ 772:∘ 768:0.0000004 764:− 759:∘ 748:ϵ 706:⁡ 697:− 691:⁡ 682:− 632:β 596:⁡ 588:∘ 574:⁡ 566:∘ 549:λ 481:multiples 419:∘ 415:0.9856003 406:∘ 360:∘ 356:0.9856474 347:∘ 302:2451545.0 299:− 202:surveying 194:astronomy 149:longitude 3035:website. 3015:website. 2653:Archived 2481:with an 2449:Sun path 2414:Ecliptic 2402:See also 2384:sundials 2372:azimuths 2343:, since 2318:analemma 2310:analemma 2304:Analemma 2288:analemma 2278:Analemma 2263:showing 2212:parallax 1507:aphelion 1475:linearly 1430:with an 1381:azimuths 976:quadrant 954:, where 220:design. 186:Sun path 145:meridian 141:transits 137:latitude 133:Sun path 119:ecliptic 89:and the 3075:Portals 2920:Bibcode 2565:Bibcode 2376:sunrise 2257:sundial 2127:0.98565 2074:0.98565 2059:0.39779 1567:is 0°. 1563:, and δ 1557:equinox 1540:At the 1457:at the 1441:, in a 1417:seasons 1395:on the 860:in the 700:0.00014 685:0.01671 679:1.00014 654:as the 485:‍ 402:357.528 343:280.460 268:J2000.0 249:Fortran 218:sundial 113:on the 81:in the 48:98°36′E 2692:  2628:  2583:  2516:  2380:sunset 2048:arcsin 1970:365.24 1944:0.0167 1897:365.24 1831:arcsin 1594:arcsin 1451:Uranus 1439:sphere 1399:. 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Index

Declination of the Sun

Phang Nga Bay
8°17′N 98°36′E / 8.283°N 98.600°E / 8.283; 98.600
sky
time
geographic location
Earth
Earth orbits
Sun
year
fixed stars
celestial sphere
ecliptic
Earth's rotation
diurnal motion
Sun path
latitude
transits
meridian
longitude
ecliptic coordinate system
equatorial coordinate system
horizontal coordinate system
solar zenith angle
solar azimuth angle
Sun path
astronomy
navigation
surveying

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